Mindat.org (original) (raw)
Locality type:
Meteorite Fall Location
Origin locality:
Notes:
Ohtani, E., Ozawa, S., Miyahara, M., Ito, Y., Mikouchi, T., Kimura, M., ... & Hiraga, K. (2011). Coesite and stishovite in a shocked lunar meteorite, Asuka-881757, and impact events in lunar surface. Proceedings of the National Academy of Sciences, 108(2), 463-466.
Classification
Species:
Stishovite
Formula:
SiO2
Confirmation
Validity:
Believed Valid
Data
Mineral Data:
Click here to view Stishovite data
Locality Data:
Data Identifiers
Mindat Occurrence Record ID:
1092635
Long-form Identifier:
1:3:1092635:4
GUID (UUID V4):
c281d455-1fd2-4f4d-936b-de44090cdfac
References
Reference Search (possible matching items)
Xirouchakis, Dimitrios, Draper, David S., Schwandt, Craig S., Lanzirotti, Antonio (2002) Crystallization conditions of Los Angeles, a basaltic Martian meteorite. Geochimica et Cosmochimica Acta, 66 (10) 1867-1880 doi:10.1016/s0016-7037(01)00892-4 | Journal (article/letter/editorial) | |
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conditions of Los Angeles, a basaltic Martian meteorite DIMITRIOS XIROUCHAKIS,1,* DAVID S. DRAPER,1 CRAIG...INTRODUCTION AND PREVIOUS WORK The basaltic Martian meteorite Los Angeles, a microgabbro, was first described...(2000a, 2000b), and Greenwood et al. (2000). This meteorite has several compositional features suggesting...Shergotty and QUE94201), and the lunar mare meteorite Asuka 881757 (Mikouchi, 2000). Los Angeles 5103...it Crystallization conditions of Los Angeles meteorite 1869 1870 D. Xirouchakis, D. S. Draper, C | ||
(1998) Abstracts. Meteoritics & Planetary Science, 33. doi:10.1111/j.1945-5100.1998.tb01327.x | Journal (article/letter/editorial) | |
Lumparn impact structure [ 1.21 represents an almost _land_-locked bay situated in the Aland main island, SW-Finland...a r y Science, Vol. 33, No. 4, Supplement, 1998 land, Spec. Paper 21, 59-97. [5] Winterhalter B. (1982)...impact-induced fracturing and brecciation. The eastern periphery of the topographic plain, covered with...magnetization [3]. This anomaly is most distinct in the eastern part of the central uplift. The seimic and gravity...certain asymmetry of the crater basin [2]. The eastern moat-rim transition is considerably shallower than | ||
(2000) Abstracts. Meteoritics & Planetary Science, 35. doi:10.1111/j.1945-5100.2000.tb01796.x | Journal (article/letter/editorial) | |
(Dhofar 007) and noncumulated (NWA 011). Results: A meteorite shower, 37 pieces weighing a total of 21,270 g...REE pattern supports a cumulate type of this meteorite also. At the other side the data of NWA 011 are...REE pattern supports a noncumulate type of this meteorite. Thus, these two meteorites belong to different...local materials and not from a widespread mix of meteorite types. From these observations we infer that the...metal grain volumetric difference between the two meteorite classes. Because of the problem of pairing meteorites |